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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>James Roberts</dc:contributor>
  <dc:creator>Fabio Lepori</dc:creator>
  <dc:date>2017</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;We used monitoring data from Lake Lugano (Switzerland and Italy) to assess key ecosystem responses to three decades of nutrient management (1983–2014). We investigated whether reductions in external phosphorus loadings (L&lt;/span&gt;&lt;sub&gt;ext&lt;/sub&gt;&lt;span&gt;) caused declines in lake phosphorus concentrations (P) and phytoplankton biomass (Chl &lt;/span&gt;&lt;i&gt;a&lt;/i&gt;&lt;span&gt;), as assumed by the predictive models that underpinned the management plan. Additionally, we examined the hypothesis that deep lakes respond quickly to L&lt;/span&gt;&lt;sub&gt;ext&lt;/sub&gt;&lt;span&gt; reductions. During the study period, nutrient management reduced L&lt;/span&gt;&lt;sub&gt;ext&lt;/sub&gt;&lt;span&gt; by approximately a half. However, the effects of such reduction on P and Chl &lt;/span&gt;&lt;i&gt;a&lt;/i&gt;&lt;span&gt; were complex. Far from the scenarios predicted by classic nutrient-management approaches, the responses of P and Chl &lt;/span&gt;&lt;i&gt;a&lt;/i&gt;&lt;span&gt; did not only reflect changes in L&lt;/span&gt;&lt;sub&gt;ext&lt;/sub&gt;&lt;span&gt;, but also variation in internal P loadings (L&lt;/span&gt;&lt;sub&gt;int&lt;/sub&gt;&lt;span&gt;) and food-web structure. In turn, L&lt;/span&gt;&lt;sub&gt;int&lt;/sub&gt;&lt;span&gt; varied depending on basin morphometry and climatic effects, whereas food-web structure varied due to apparently stochastic events of colonization and near-extinction of key species. Our results highlight the complexity of the trajectory of deep-lake ecosystems undergoing nutrient management. From an applied standpoint, they also suggest that [&lt;/span&gt;&lt;i&gt;i&lt;/i&gt;&lt;span&gt;] the recovery of warm monomictic lakes may be slower than expected due to the development of L&lt;/span&gt;&lt;sub&gt;int&lt;/sub&gt;&lt;span&gt;, and that [&lt;/span&gt;&lt;i&gt;ii&lt;/i&gt;&lt;span&gt;] classic P and Chl &lt;/span&gt;&lt;i&gt;a&lt;/i&gt;&lt;span&gt; models based on L&lt;/span&gt;&lt;sub&gt;ext&lt;/sub&gt;&lt;span&gt; may be useful in nutrient management programs only if their predictions are used as starting points within adaptive frameworks.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/j.jglr.2017.01.008</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>International Association for Great Lakes Research</dc:publisher>
  <dc:title>Effects of internal phosphorus loadings and food-web structure on the recovery of a deep lake from eutrophication</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>